Use of clay-mineral alteration patterns to define syntectonic permeability of joints (cleat) in Pennsylvania anthracite coal
- 22 February 1999
- journal article
- Published by Elsevier
- Vol. 263 (1-4) , 123-136
- https://doi.org/10.1016/s0040-1951(96)00019-4
Abstract
No abstract availableKeywords
This publication has 19 references indexed in Scilit:
- Late Permian age of NH4-bearing illite in anthracite from eastern Pennsylvania: Temporal limits on coalification in the central AppalachiansGSA Bulletin, 1994
- Inorganic nitrogen in anthracite from eastern Pennsylvania, USAInternational Journal of Coal Geology, 1993
- BRINE MIGRATIONS ACROSS NORTH AMERICA—THE PLATE TECTONICS OF GROUNDWATERAnnual Review of Earth and Planetary Sciences, 1990
- Hydrothermal alteration in anthracite from eastern Pennsylvania: Implications for mechanisms of anthracite formationGeology, 1990
- The relationship of coal optical fabrics to Alleghanian tectonic deformation in the central Appalachian fold-and-thrust belt, PennsylvaniaGSA Bulletin, 1989
- From field data to fracture network modeling: An example incorporating spatial structureWater Resources Research, 1987
- Fluid flow through rock joints: The effect of surface roughnessJournal of Geophysical Research, 1987
- Mineralogic domains in very low grade pelitic rocksGeology, 1987
- Surface morphology on cross-fold joints of the Appalachian Plateau, New york and PennsylvaniaTectonophysics, 1984
- Permeability of crystalline and argillaceous rocksInternational Journal of Rock Mechanics and Mining Sciences, 1980